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Kermadec Trench: Like pieces of a jigsaw puzzle…

The views expressed are those of the author and are not necessarily those of Scientific American.


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A specimen photograph of Coryphaenoides yaquinae. If confirmed with more detailed study at Te Papa, this will be the first proven record in New Zealand waters. Photo credit: NIWA/University of Aberdeen.

A specimen photograph of Coryphaenoides yaquinae. If confirmed with more detailed study at Te Papa, this will be the first proven record in New Zealand waters. Photo credit: NIWA/University of Aberdeen.

Today saw retrieval of the two landers and fish trap from depths of 5000-5500m. This is still on the abyssal plain between the Kermadec Ridge and Kermadec Trench, but is starting to become a steeper slope as depths drop away towards the Trench. The hadal lander was the first aboard, and with it came video footage of a rough and rocky seafloor. Unfortunately the camera power failed after just two hours, and in that time very few fish were seen. The abyssal lander however, worked well and showed rattails, cusk eels, and large penaid shrimps-although none appeared abundant. The fish trap caught only a single fish, but there was no disappointment as it was another new record for the New Zealand region, believed to be Coryphaenoides yaquinae. There was also a good catch of amphipods.

The specimens of Coryphaenoides armatus from yesterday and Coryphaenoides yaquinae today are helping to piece together our understanding of the distribution of deep-sea fishes. Although C. armatus was known to occur, the specimens have confirmed it is relatively abundant in deep New Zealand areas (based on camera work). C. yaquinae is known from the North Pacific, (including the Japan and Mariana Trenches) and off Chile and Peru. But this is the first record in the Southwest Pacific, and proves a widespread Pacific rim distribution. For all of us onboard these are exciting results.

Preparing the Hadal Lander. Alan Jamieson (left) sets up the camera, while Niki Lacey (centre) and Heather Ritchie (right) (both PhD students at the University of Aberdeen) secure an amphipod trap to the leg of the lander. Photo credit: NIWA/University of Aberdeen.

Preparing the Hadal Lander. Alan Jamieson (left) sets up the camera, while Niki Lacey (centre) and Heather Ritchie (right) (both PhD students at the University of Aberdeen) secure an amphipod trap to the leg of the lander. Photo credit: NIWA/University of Aberdeen.

Amphipods haven’t featured much in the reports to date. But we are now approaching depths where things get interesting. The main species we have seen so far is Eurythenes gryllus, a worldwide species, and the second largest only to the “supergiant” Alicella. There was a good catch today, but we expect numbers to decrease as we go deeper onto the Trench. While in other trench systems Eurythenes is found as deep as 7000m, in the Kermadec Trench it hasn’t been found past 6000m, where we see other amphipod species dominate. We don’t know why, although one possibility being studied on this trip through genetic studies is the possibility that there is more than one species with different depth ranges, but they look the same-so-called “cryptic” species.

This afternoon we deployed the gear at around 6000m, and if the weather holds we hope to go deeper still the following day – into the Trench proper – to improve our knowledge of how faunal communities change in the deep.

Previously in this series:

Kermadec Trench: Cook, Kermadec and Kaharoa
Previous research in the Kermadec Trench
Kermadec Trench: Scuttling your Assets
Kermadec Trench: Boring eels
Kermadec Trench: The Cosmopolitan Rattail
Kermadec Trench: The deep-water womble

Malcolm Clark About the Author: Dr. Malcolm Clark is a Principal Scientist (Deepwater Fisheries) at the National Institute of Water and Atmospheric Research (NIWA) in Wellington, New Zealand. He is specialized in deep-sea fish and fisheries, seamount ecology, and the impacts of human activities. Dr. Clark was a lead principal investigator for the Census of Marine Life program on Seamounts (2005-11), and currently heads NIWA research programs on the biology and ecology of deep-sea communities (including seamount, hydrothermal vent, canyon and trench habitats).

The views expressed are those of the author and are not necessarily those of Scientific American.





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